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phy excursions and a good lead pencil on e<tui ucm 
trip. 

Excursion note books must be neatly kept, and will be ex¬ 
amined in the field by the instructor from time to time 
to see that the notes are entered fully and carefully. 


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University Hall What is the distance from the lake?. 


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How is Madison situated with reference to Lake Mendota? 
























nona and Lake Mendota? 


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Is the surface material transported? 

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What has become of the material ? 



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dimensions and 1 inch equal 60 feet in horizontal dimensions. 
Use the symbols shown on inside of front cover. 





Mendota limestone. 
Potsdam sandstone. 













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fresh inner surface? . Explain 


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was it deposited? 


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The slope of the fan in feet per mile, is . The 

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Has it abandoned channels on the surface ?.Describe 



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AVhat economic resource, much used by man in cool temperate 
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Fig. 4. Map of region near Lakes Wingra and Monona (after 
U. S. Geol. Survey. Contour interval 20 feet. 








































(d) Wave-built; 



































(e) Made by disintegration of older rock in place; 


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List the rocks found here according to the following table. 























Along 1 Drive Be sure and follow exact location on your 
in Swamp map. Examine the whitish material along the 

drive. Tell why it may or may not be: (a) till;. 


(b) lake clay; 



































Can shells he found in the canal along the drive 



Uses ? 


What name may be applied to the dark surface material in the 


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the small stones have bad on the large ones and 



























What is the direction of the scratches or striae 





Is it a lake deposit ? 


























Is it the unassorted product of crushing and grinding 



Write down the differences and similarities of material here 
and at the gravel pit in the following table. 




















Assorted or not 





Recent soil 

Recent marl 

Recent swamp deposits 



































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contain striated bowlders? Prove that these are glacial er¬ 
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Suggest an explanation of this, 


Hill Near What is the shape of this hill? 

Sun Prairie . Its tren d» . 

Road 

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How do you distinguish a glacer worn pebble from a water-worn 



How could you distinguish it from a drumlin? 
















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at random. What percentage are (a) limestone? . 

(b) sandstone?.(c) igneous and metamorphic 


Account for the percentage of each 








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Look in the fields next crossed for evidence bearing on this 


Describe it. 


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k modified the slopes of the ridge in 




















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Fig. 7. Cross section from City stone quarry to University Bay (Col¬ 
lege Hills) moraine. Vertical scale three times the horizontal. 


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ITas tho relief here been increased or decreased by glaciation? 


















How much for the quarry hill?. 

How much for the hill upon which you are standing? 



How much do they vary in depth and size? 


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Of vvliat uses to man are gravel deposits like those seen today" 


Are they more or less useful than till deposits? 


on 

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At Canoe In pre-glacial time the local drainage was prob- 
Portage ably as shown in Fig. 8. Picnic Point was then a 



spur between Middleton River and University Pay Creek. What 
kind of rock is exposed here (Fig. 16) ? . 








Place in geological column?. What effect 

will this outcrop have upon future modification of this point ? 



Ro ck 


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Fig. 9. Cross section of University Bay. Vertical scale five times the 

horizontal. 



What is the origin of this material? 



























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Ts the process still going on? 


Evidence 





























End of What evidence do you see that the end of the point 

POlTlti p /-w^n_d d -P <-* + r*>» "f r\ fllO 11 OVtll P,flSt ? • ••••• 


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Compare the percentage of bowlders found here with percentage 
at last stop. Ex P’ ain . 


Is this coast then due to constructional or destrnctional pro- 
, .Why? . 

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Report Write a brief geological history of the point, follow 
ing this outline. 

1. Pre-glacial deposition; 2. Pre-glacial erosion; 3. Gla¬ 
ciation; 4. Post-glacial erosion. 



















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COVE NORTHWEST OF PICNIC POINT 


Features of Shore Line Transportation and Deposition. 




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Is erosion or deposition dominant here? 





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What determines the size of material that can he carried? . 


















What is the effect of transportation upon the transported ma- 




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sand spit stippled. 











































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Is this the usual rule? .What effect would the com- 










o 

CO 



Is there any evidence of an abandoned beach in front of this cliff? 


What process dominates in the lagoon ?. 

What kinds of deposits are accumulating there? 






























Outline the future history of the bay west of the bar 


On the Drive Outline the history of this drive 







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Print the following names on Fig. 10; Old shore line, first bar, 
submerged bar, Indicate by the letter “C” several places where 
cliff cutting is going on; by the letter “D” places where deposi¬ 

tion is in progress. 
























Estimate the number of acres that University Hay has lost 

through natural modification.acres. What has 

man done to modify it still further .. 










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On Boat While the boat is slowly skirting the cliff answer 
the following. What processes are important in the formation 


Which is the most important ?. 

Why are there irregularities in the cliff taee ? 



What becomes of the material that falls or is worn from the cliff ? 






















on 

ain 










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What was the origin of the material forming the bar? 


If cutting continues on the rock cliff and on the till cliff 200 yards 
to the east, what will become of this lagoon?. 


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Wlmt is the kind of rock forming the cliff at this place ? 
























___ 


jtfi/e 



Fig. 11. Map of Maple Bluff and eastern part of Lake Mendota 
(after U. S. Geol. Survey). Contour interval above and below 
lake level 20 feet. 















If it is of one formation why are there irregularities in the cliff 


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Kind of rock (sandstone, limestone, or shale) ? 


Do they vary in thickness?. 

What peculiarity of color has it?. 

What name is applied to it (Fig. 16)? . 

If you have seen this same formation before on any of your ex- 




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At South Madison How high is this ridge above sea level 
Railway Cut (Fig. 4) ? Above Lake Monona?. 


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Bridge over that two, three, and four contours are superimposed 
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in Fig. 4 is at the bridge and not on the hill top). 

What thickness of rock is exposed here? . 


the cut (Fig. 12) ?. 

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sandstone ? 






















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Draw a profile showing the relation of pre-glacial 



Is the glacial till thinner or thicker on this hill than in the 
valley to the north ? . 



has been modified since its formation. 












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a glacial deposit 1 ? . 

AVhat evidence of each would you look for? 
















Fig. 14. Map of region near Esther Beach and Round Top (after 

U. S. Geol. Survey). 







































Along 1 Road Describe the material exposed along the road. 



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How does this hill differ in composition, elevation and outline 
from the hill to the west which has the rock cut (excursion 11) ? 





What has man done to destroy the lakes and swamps 























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Buildings (a) the name of rock or other material, (b) 

class of rock, (c) where obtained; (d) how affected by weath- 



















108 


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PART OF THE UNIVERSITY CAMPUS 


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Hall at the regular laboratory hour. Until the dome of the new 
capitol is completed it will be necessary to use the roof of Uni¬ 
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elevations of any other conspicuous hills, or summits which are 
visible ... 



Tell where you have seen each successive overlying formation 
shown in Fig. 16, arranging them in order in the following 
table, beginning at the bottom. 




















■a _= 







































































Make a rough cross-section from Eagle Heights to Maple Bluff, 
showing topography and rock formations. 



Locate one which you have 



























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Tell where you entered the Driftless Area on an excursion of 
each semester... 


What can you say of the origin or history of Eagle Heights, 
University Hill, hill southwest of Esther Beach, and the hdl 



What is the source of its water supply? 





























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shoes or boots should be worn. Except by special permission 
none but members of the class may go on this excursion. 


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western station at Madison above sea level (Fig. 5) ? . 

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(b) lakes and swamps or none (partly-filled Lake Wingra) ; 










Fig. 18. Geological map of the region between Madison and Blue 
Mounds (after Wisconsin Geological and Natural History Survey). 
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(e) glacial till or stratified gravel or residual soil. 


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Fig. 20. Contour map of the region near Blue Mound (after 
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Review and summary of matters seen on train. 




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of the glaciation ? . 


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Fig. 23. Geological map of the region between Madison and 
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Between Madison and the Wisconsin River we ascend the back 
slope of a cuesta and then descend its escarpment. (Elevation 
at Madison, 850; Waunakee, 925; Dane, 1080; Lodi, 860; Okee, 
810; Wisconsin river, 765 feet). What railway station is 


nearest the crest (Fig. 23). What station 

at the base of the escarpment?.What rock for- 

• mation is the euesta-maker (Fig. 23)? *.How 



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actly where you crossed belts of (a) terminal moraine, (b) 
ground moraine, (c) outwash, (d) lake clay, (e) sand dunes. 



















(1 what topography and drift material you saw in each case. 




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'Fry to discover where we cross the westernmost recessional (ter¬ 
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154 



What geological formations (Pleistocene, Cambrian, etc.) are 
seen between Madison and Devils Lake (Fig. 23) ? 


Make a list of physiographic processes which are especially well 
illustrated along the route, noting the locality where seen. 



Reasons ? 

























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Monad nock in New Hampshire?. 

Why is it higher than the surrounding country? 



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What is an unconformity? 


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Was the Baraboo Range glaciated ? n 

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ridge, and absent from the steeper slopes? 


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Fig. 26. Hydrographic map of Devils Lake (after F. T. 
Thwaites). Surface 955 to 959 feet above sea level. Sub¬ 
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Is there more talus in the glaciated region than in the Driftless 
Area?.Why? . 





Fig. 27. Cross section of Devils Lake gap. Depth of glacial filling 
estimated from adjacent wells. Vertical and horizontal scales the 
same. 




































Has the lake an outlet? .How does the water 



Reasons for answer 


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the terminal moraine? 





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170 




taken from Madison as there is no opportunity to get meals at 
the Dalles and no time to purchase anything in Kilbourn before 
the boat leaves. Except by special permission, none but mem¬ 
bers of the class may go on this excursion. Wear high shoes or 
boots as there is some walking over s'tony and sandy ground. 





Yahara River and faint recessional moraine topography east of 













of Darwin. Draw profiles of some of the drumlins seen 


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Fig. 28. Geological map of the region between Madison and the 
Dalles (after Wisconsin Geological and Natural History Sur¬ 
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into Green Bay, and Lake Michigan. Is this apparently a busy 
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it were in Germany or in China 



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Does jointing influence the form of the banks ? 
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At Louis Describe and explain the features of the Driftless 
Bluff Area and the glaciated region from the top of the bluff. 










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planations outlined above and any other points discussed by the 
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mg at a time to tie announced. I he expense is 96 cents for railway 
and street car fare, plus a possible 50 cents for carriage hire. 
Lunch should be taken from Madison. Each member of the 
class will be provided with copies of the Madison, Sun Prairie, 
and Waterloo Quadrangles. 


On Train Between Madison and Waterloo make notes on the 
topographic forms seen and the material exposed in railway cuts. 
Determine the direction of ice movement from Fig. 17 and 
note its relationship to direction of axes of drumlins. Upon the 
three topographic maps, outline in pencil as many drumlins as 


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On Train Study the topographic maps, determining from Fig. 
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borders on your map and make notes on the topographic 
forms there and in the ground moraine. Look for evidence of 
lake deposits and of outwash gravels at and west of Middleton. 


to « 


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Excursion 23 



Denser, Sparta, Waukon, Elkader, Lancaster, Mineral Point, 
Galena, and Cross Plains Quadrangles and of Mississippi River 
charts 125 to 130 (one inch to one mile) and charts 161 to 173 
(1:20,000 scale) will be provided. 


Madison to Car window observations of the physiographic 
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